ApRES time series from Roi Baudouin Ice Shelf, 2016/02-2017/01 ...

The ApRES (Brennan et al., 2014; Nicholls et al., 2015) was deployed from January to December in 2016 on the RBIS about 90 km from the ice shelf front and 5 km seaward from the grounded ice on the fast-flowing portion of the West Ragnhild glacier, which is the third largest outlet glacier along the...

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Bibliographic Details
Main Authors: Sun, Sainan, Pattyn, Frank
Format: Dataset
Language:English
Published: PANGAEA 2024
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.964065
https://doi.pangaea.de/10.1594/PANGAEA.964065
id ftdatacite:10.1594/pangaea.964065
record_format openpolar
spelling ftdatacite:10.1594/pangaea.964065 2024-03-31T07:52:29+00:00 ApRES time series from Roi Baudouin Ice Shelf, 2016/02-2017/01 ... Sun, Sainan Pattyn, Frank 2024 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.964065 https://doi.pangaea.de/10.1594/PANGAEA.964065 en eng PANGAEA https://dx.doi.org/10.1029/2019gl083881 https://dx.doi.org/10.1049/iet-rsn.2013.0053 https://dx.doi.org/10.1002/2014jf003246 https://dx.doi.org/10.3189/2015jog15j073 https://dx.doi.org/10.1126/science.1235798 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 ApRES Ice shelf NECKLACE DATE/TIME netCDF file netCDF file File Size Multiple investigations dataset Dataset 2024 ftdatacite https://doi.org/10.1594/pangaea.96406510.1029/2019gl08388110.1049/iet-rsn.2013.005310.1002/2014jf00324610.3189/2015jog15j07310.1126/science.1235798 2024-03-04T12:41:01Z The ApRES (Brennan et al., 2014; Nicholls et al., 2015) was deployed from January to December in 2016 on the RBIS about 90 km from the ice shelf front and 5 km seaward from the grounded ice on the fast-flowing portion of the West Ragnhild glacier, which is the third largest outlet glacier along the Dronning Maud Land Coast (Callens et al., 2014). The ice thickness at the site was ∼300 m in the trough of a channel (Drews, 2015) but increases up to 600 m in the grounding zone upstream, and ice flow velocities in this region range between 250 and 300 m/a (Rignot et al., 2013). By transmitting an electromagnetic signal and receiving the echo, the radar system can detect the ice base (ice-ocean interface) as well as relatively weak internal reflecting layers that are due to changes in ice permittivity. Between two consecutive measurements, the relative vertical motion of internal layers and the base can therefore be tracked. The displacements of the internal layers determine how the thickness of the column ... Dataset Dronning Maud Land Ice Shelf DataCite Metadata Store (German National Library of Science and Technology) Dronning Maud Land Roi Baudouin ENVELOPE(24.461,24.461,-70.438,-70.438)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic ApRES
Ice shelf
NECKLACE
DATE/TIME
netCDF file
netCDF file File Size
Multiple investigations
spellingShingle ApRES
Ice shelf
NECKLACE
DATE/TIME
netCDF file
netCDF file File Size
Multiple investigations
Sun, Sainan
Pattyn, Frank
ApRES time series from Roi Baudouin Ice Shelf, 2016/02-2017/01 ...
topic_facet ApRES
Ice shelf
NECKLACE
DATE/TIME
netCDF file
netCDF file File Size
Multiple investigations
description The ApRES (Brennan et al., 2014; Nicholls et al., 2015) was deployed from January to December in 2016 on the RBIS about 90 km from the ice shelf front and 5 km seaward from the grounded ice on the fast-flowing portion of the West Ragnhild glacier, which is the third largest outlet glacier along the Dronning Maud Land Coast (Callens et al., 2014). The ice thickness at the site was ∼300 m in the trough of a channel (Drews, 2015) but increases up to 600 m in the grounding zone upstream, and ice flow velocities in this region range between 250 and 300 m/a (Rignot et al., 2013). By transmitting an electromagnetic signal and receiving the echo, the radar system can detect the ice base (ice-ocean interface) as well as relatively weak internal reflecting layers that are due to changes in ice permittivity. Between two consecutive measurements, the relative vertical motion of internal layers and the base can therefore be tracked. The displacements of the internal layers determine how the thickness of the column ...
format Dataset
author Sun, Sainan
Pattyn, Frank
author_facet Sun, Sainan
Pattyn, Frank
author_sort Sun, Sainan
title ApRES time series from Roi Baudouin Ice Shelf, 2016/02-2017/01 ...
title_short ApRES time series from Roi Baudouin Ice Shelf, 2016/02-2017/01 ...
title_full ApRES time series from Roi Baudouin Ice Shelf, 2016/02-2017/01 ...
title_fullStr ApRES time series from Roi Baudouin Ice Shelf, 2016/02-2017/01 ...
title_full_unstemmed ApRES time series from Roi Baudouin Ice Shelf, 2016/02-2017/01 ...
title_sort apres time series from roi baudouin ice shelf, 2016/02-2017/01 ...
publisher PANGAEA
publishDate 2024
url https://dx.doi.org/10.1594/pangaea.964065
https://doi.pangaea.de/10.1594/PANGAEA.964065
long_lat ENVELOPE(24.461,24.461,-70.438,-70.438)
geographic Dronning Maud Land
Roi Baudouin
geographic_facet Dronning Maud Land
Roi Baudouin
genre Dronning Maud Land
Ice Shelf
genre_facet Dronning Maud Land
Ice Shelf
op_relation https://dx.doi.org/10.1029/2019gl083881
https://dx.doi.org/10.1049/iet-rsn.2013.0053
https://dx.doi.org/10.1002/2014jf003246
https://dx.doi.org/10.3189/2015jog15j073
https://dx.doi.org/10.1126/science.1235798
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.1594/pangaea.96406510.1029/2019gl08388110.1049/iet-rsn.2013.005310.1002/2014jf00324610.3189/2015jog15j07310.1126/science.1235798
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